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首页> 外文期刊>Current Science: A Fortnightly Journal of Research >Discovery of volcanic ash bed from the basal Subathu Formation (Late Palaeocene-Middle Eocene) near Kalka, Solan District (Himachal Pradesh), Northwest Sub-Himalaya, India
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Discovery of volcanic ash bed from the basal Subathu Formation (Late Palaeocene-Middle Eocene) near Kalka, Solan District (Himachal Pradesh), Northwest Sub-Himalaya, India

机译:在印度喜马拉雅山西北部索兰区(希马克萨尔邦)卡尔卡附近的基底苏巴图组(晚新世-中始新世)发现火山灰床

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Discovery of 1.5 m thick volcanic ash bed is reported from the basal part of the Late Palaeocene–Middle Eocene Subathu Formation exposed along the Koshaliya river near Kalka (Solan District) in the foothills of Himachal Pradesh. The ash bed represents the oldest volcanic ash horizon from this part of the Himalayan Foreland Basin. The ash is fine-grained and consists mostly of kaolinite with trace quantities of glass shards, euhedral and angular beta-quartz, sanidine, zircon, biotite and anatase. Ithas high concentrations of Al2O3 as well as incompatible elements (Zr, Nb, Th and Y), and high loss on ignition. Based on lithological as sociation, field characters, mineralogy and geochemistry, the ash bed has been identified as tonsteins of a volcanicorigin. The stratigraphic position and thickness of the ash bed indicate a significant volcanic event during the Early Eocene.
机译:据报道,在喜马al尔邦山麓的卡尔卡(索兰区)附近的科沙里亚河沿河,古新世-中始新世苏巴图组的底部发现了1.5 m厚的火山灰床。灰床代表了喜马拉雅前陆盆地这一部分最古老的火山灰层。灰是细粒的,主要由高岭石和痕量的玻璃碎片,正反面和角β石英,山铁矿,锆石,黑云母和锐钛矿组成。它具有高浓度的Al2O3以及不相容的元素(Zr,Nb,Th和Y),并且燃烧时的损失高。根据社会学,田野特征,矿物学和地球化学的岩性,火山灰床已被确定为火山古菌素的tonsteins。灰烬层的地层位置和厚度表明,在始新世早期有重大的火山事件。

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